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India's Sedimentary Basins: Subsurface Insights        39



            2.2.3 CAMBAY BASIN

            Cambay is a Category I basin with commercial discovered in-place.
            The area geographically overlaps with the state(s) of Gujarat, Rajasthan.









































             Source: DGH Internal                               Source: DGH Internal

            The basin is characterized primarily by siliciclastic  Miocene  plays  (Babaguru)  are  proved  to  be
            rift-fill sediments, situated in the western region  potential  reservoirs  of  oil  and  gas  in  southern
            of Indian peninsula. The basin is endowed with  onland part of the basin and the offshore area
            most  matured  petroleum  provinces  of  India  that extends into the Gulf of Cambay.
            with  major  producing  fields  and  88%  of  total
            hydrocarbons already discovered.                  Paleogene  plays  (Akholjuni,  Gandhar)  and
                                                              Mesozoic remain the key focus area of the basin.
            The Cambay basin, though extensively exploited,
            is still under active exploration for deep-seated   •   Hydrocarbon prospectivity and Basin
            plays.  Commercial  hydrocarbon  occurrences          maturity:
            are spread over different stratigraphic intervals   In  the  basin,  7  plays  exist  within  Basement,
            ranging  from  the  oldest  sediments,  including   Paleocene,  Eocene  and  Miocene.  Petroleum
            Deccan Trap volcanics of Cretaceous-Paleocene     system  was  modelled  in  3D  basis  adequate
            to the youngest sediments of Miocene. Several     datasets.
            oil and gas fields have been discovered, out of
            which  two-third  of  the  discoveries  has  been  Onland  sub-basin  has  a  total  hydrocarbon  in-
            made in Middle Eocene.                            place of 2,054 MMTOE. This includes discovered
                                                              in-place of 1,801 MMTOE and undiscovered risked
            Cambay shale of Paleocene is the major source     in-place of 253 MMTOE. The discovered in-place
            rock charging Middle Eocene reservoirs of Kalol   is under commercial production. The basin has
            (North and Central) and Hazad (Southern) deltaic   12.3%  of  total  in-place,  potential  to  be  explored
            reservoirs  with  Tarapur  (Oligocene)  acting  as   and discovered.
            the regional cap rock. During later exploration,
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